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�u <br /> " r►uAM <br /> ✓tom—/�A <br /> Working to Restore Nature <br /> Previous Environmental Work <br /> In May and June 1988, RESNA (formerly Applied GeoSystems) collected nine soil samples <br /> from test pits excavated near the dispenser islands and observed removal of three 12,000- <br /> gallon tanks at the site (Applied GeoSystems, July 8, 1988) The tanks were replaced with <br /> two gasoline tanks, which are presently at the site Soil samples collected from the test pits <br /> and beneath the tanks contained gasoline hydrocarbons The excavation was terminated due <br /> to the proximity to the road and existing structures Hydrocarbon-containing soil was left <br /> in place <br /> Nineteen soil borings have been drilled at or near the site Thirteen of these borings were <br /> converted into groundwater monitoring wells, four were converted into vapor extraction <br /> wells, one into a pumping test well, and one soil boring was backfilled The initial five <br /> monitoring wells were installed in January and February 1990 and have been predominantly <br /> dry since October 1990 Three additional wells and the four vapor extraction wells were <br /> installed in March 1992 The final five monitoring wells were installed offsite in August <br /> 1992 and delineate dissolved hydrocarbons in groundwater (RESNA, December 16, 1992) <br /> In March 1992, a vapor extraction test was performed at the site (RESNA, June 29, 1992), <br /> and in August 1992, a groundwater pumping test was performed onsite (RESNA, May 4, <br /> 1993) <br /> REGIONAL GEOLOGY AND HYDROLOGY <br /> Unocal Service Station 6981 is in the Central Valley geomorphic province of California, <br /> which is a northwestward-trending, asymmetric structural trough that has been filled with <br /> 6 to 10 miles of sediment ranging in age from Jurassic to Holocene (Page, 1986) The <br /> topographic surface is nearly flat with a slight westward slope Based on an extrapolation <br /> of a geological map prepared by Marchand and Atwater (1979), sediments beneath the site <br /> consist of Quaternary alluvial deposits of the Modesto Formation, which were deposited by <br /> the Mokelumne River The nearest surface stream is the Calaveras River which trends east <br /> and west approximately 1,800 feet southeast of the site <br /> PRESENT INVESTIGATION <br /> The work was performed according to RESNA's Work Plan 38032-14W (RESNA, August <br /> 18) and Site Safety Plan 38032-93S (RESNA, January 1993) Details of the drilling <br /> operations, soil sampling, and laboratory analyses are presented below Our field methods <br /> are described in an attachment to this report Copies of the Chain of Custody Records and <br /> laboratory reports for soil samples are attached <br />. 1214dcam/38032-14 2 <br />